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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F10%3A00000042%21RIV11-GA0-00025798
rdf:type
skos:Concept n13:Vysledek
dcterms:description
Lithium data are presented for plutonic rocks from the Western Carpathians, Slovakia, that were generated throughout the complete Variscan orogenic cycle. I-type granites show a limited range of δ7Li, contrasting with the large variations found in S-type granites and orthogneisses of distinct ages. An exclusively heavy Li isotope signature (δ7Li > 4.7‰) found in A-type granites rules out several commonly accepted petrogenetic scenarios. It most probably reflects a derivation of A-type granites from a mantle wedge modified by slab-derived fluids. Mafic rocks (gabbros and diorites), associated with occurrences of granites, are uniformly Li-rich and isotopically light (< - 0.5‰), precluding a direct derivation from the mantle. These signatures testify to their cumulate origin. The presumed dichotomy between the sources and processes leading to generation of S- and I-type granitic magmas does not seem to be reflected by Li isotope signatures in a simple and globally valid manner. Lithium data are presented for plutonic rocks from the Western Carpathians, Slovakia, that were generated throughout the complete Variscan orogenic cycle. I-type granites show a limited range of δ7Li, contrasting with the large variations found in S-type granites and orthogneisses of distinct ages. An exclusively heavy Li isotope signature (δ7Li > 4.7‰) found in A-type granites rules out several commonly accepted petrogenetic scenarios. It most probably reflects a derivation of A-type granites from a mantle wedge modified by slab-derived fluids. Mafic rocks (gabbros and diorites), associated with occurrences of granites, are uniformly Li-rich and isotopically light (< - 0.5‰), precluding a direct derivation from the mantle. These signatures testify to their cumulate origin. The presumed dichotomy between the sources and processes leading to generation of S- and I-type granitic magmas does not seem to be reflected by Li isotope signatures in a simple and globally valid manner.
dcterms:title
Fingerprinting sources of orogenic plutonic rocks from Variscan belt with lithium isotopes and possible link to subduction-related origin of some A-type granites Fingerprinting sources of orogenic plutonic rocks from Variscan belt with lithium isotopes and possible link to subduction-related origin of some A-type granites
skos:prefLabel
Fingerprinting sources of orogenic plutonic rocks from Variscan belt with lithium isotopes and possible link to subduction-related origin of some A-type granites Fingerprinting sources of orogenic plutonic rocks from Variscan belt with lithium isotopes and possible link to subduction-related origin of some A-type granites
skos:notation
RIV/00025798:_____/10:00000042!RIV11-GA0-00025798
n3:aktivita
n12:P n12:I n12:Z
n3:aktivity
I, P(GA205/07/0992), Z(MZP0002579801)
n3:cisloPeriodika
1-2
n3:dodaniDat
n11:2011
n3:domaciTvurceVysledku
n14:7243111 n14:2239086
n3:druhVysledku
n10:J
n3:duvernostUdaju
n17:S
n3:entitaPredkladatele
n16:predkladatel
n3:idSjednocenehoVysledku
259229
n3:idVysledku
RIV/00025798:_____/10:00000042
n3:jazykVysledku
n6:eng
n3:klicovaSlova
lithium isotopes,neodymium isotopes,granitic typology,lower crust,subduction,A-typegranite,Western Carpathians
n3:klicoveSlovo
n7:granitic%20typology n7:lower%20crust n7:A-typegranite n7:subduction n7:neodymium%20isotopes n7:lithium%20isotopes n7:Western%20Carpathians
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[CC59ADCAF41A]
n3:nazevZdroje
Chemical Geology
n3:obor
n8:DD
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
5
n3:projekt
n18:GA205%2F07%2F0992
n3:rokUplatneniVysledku
n11:2010
n3:svazekPeriodika
274
n3:tvurceVysledku
Wiechert, Uwe Magna, Tomáš Kohút, Milan Janoušek, Vojtěch Oberli, Felix
n3:wos
000279094700009
n3:zamer
n5:MZP0002579801
s:issn
0009-2541
s:numberOfPages
14